Page 104 - General Knowledge
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     GENERAL KNOWLEDGE                                                                               2019
              There are two important layers in the ionosphere viz. E layer or Kennelly Heavy side layer
                that reflects the medium radio waves, thus helping in short distance radio communication
                and F layer or Appleton layer that reflects the short radio waves and helps in long distance
                radio communication.
              The outermost layer of the Earth‘s atmosphere is known as the Exosphere. It is so highly
                rarefied a region that its boundary is not clear.
            Lithosphere
              The lithosphere is an  Earth‘s  outermost  layer,  composed  of  rocks in  the  crust  and  upper
                mantle that behave as brittle solids.
              The rigid lithosphere sits on the top of the asthenosphere, a layer of the mantle in which
                rocks are hot and deformable.
              The lithosphere is the solid, rocky crust covering the entire planet. This crust is inorganic and
                is composed of minerals.
              It covers the entire surface of the earth from the top of Mount Everest to the bottom of the
                Mariana Trench.
              The actual thickness of the lithosphere varies considerably, and can range from roughly 40
                km to 280 km.
              Earth‘s lithosphere includes the crust and the uppermost mantle, which constitute the hard
                and rigid outer layer of the Earth.
              The lithosphere is subdivided into tectonic plates.
              The  lithosphere  ends  at  the  point  when  the  minerals  in  the  earth‘s  crust  begin  to
                demonstrate viscosity and fluid behaviors.
            Rocks
              The earth‘s crust is formed of mineral materials called rocks.
              The  rocks  which  form  the  substructure  of  our  lithosphere  are  grouped  into  three  broad
                categories:
            Igneous Rocks
              Igneous rocks are formed by the solidification of molten magma from the interior of the earth.
              About 95% of the earth‘s crust is made of this type of rock. In fact, all other types of rocks
                originate from these rocks, and therefore, they are also called primary rocks.
              Igneous rocks are of three types.
            Characteristics of Igneous Rocks
              The igneous rock does not contain layers.
              They are without fossils and the upper part of the rock contains joints.
              They are formed by volcanic lava.
              They are crystalline rocks and impervious rocks.
              They are massive and the weathering effect is difficult over them.
              They are primary rocks of the crust, hence are also called the primary rocks.
            Sedimentary Rocks
              These rocks are formed from the sediment deposits on the ocean beds.
              They  comprise  only about  5%  of  the earth‘s  crust,  but  cover  about  75%  of  the  total land
                surface.
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